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Dry soil diurnal quasi-periodic oscillations in soil 222Rn concentrations
Institution:1. Institute of Earth Sciences, University of Iceland, Reykjavik, Iceland;2. NERC Isotope Geosciences Facilities, British Geological Survey, Nottingham NG12 5GG, UK;3. Dpt of Anaytical and Environmental Geochemistry (AMGC), Vrije Universiteit Brussel (VUB), Pleinlaan 2, 1050 Brussels, Belgium;4. Max Planck Institute for Chemistry, Hahn-Meitner-Weg 1, 55128 Mainz, Germany;5. LOCEAN, Sorbonne Universités, UPMC/CNRS/IRD/MNHN, Paris, France
Abstract:222Rn concentrations have been monitored during the dry season in August 2009 and August 2010, in a reworked alluvial-pyroclastic soil of the Pietramelara Plain, in Southern Italy, with the aim of determining the role of atmospheric factors in producing the quasi-periodic oscillations in soil 222Rn concentrations reported in the literature. In this study we present the results of a detailed analysis and matching of soil 222Rn concentrations, meteorological and solar parameters where the observed oscillations feature a characteristic behavior with second order build-up and depletion limbs, separated by a daily maximum and minimum. All these features are clearly shown to be tied to sunrise and sunset timings and environmental radiative flux regimes. Furthermore, a significant, and previously unreported, second order correlation (r2 = 0.73) between daily maximum hourly global radiation and the daily range of soil 222Rn concentrations has been detected, allowing estimates of the amplitude of these oscillations to be made from estimated or measured solar radiation data. The correlation has been found to be valid even in the presence of persistent patchy daytime cloudiness. In this case a daytime prolongation of the night-time build up stage and an attenuation or even suppression of daytime depletion is observed (a previously unreported effect). Neither soil cracking, nor precipitation, both suggested in some studies as causative factors for these oscillations, during the dry season appear to be necessary in explaining their occurrence. We also report the results of an artificial shading experiment, conducted in August 2009, that further support this conclusion. As soil 222Rn concentrations during the dry season show a characteristic daily cycle, radon monitoring in soils under these conditions necessarily has to be gauged to the timings of the daily maximum and minimum, as well as to the eventual occurrence of cloudiness and to its related effects, in order to avoid erroneous conclusions.
Keywords:Solar radiation  Planetary boundary layer processes  Dry season quasi-periodic oscillations
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